Abstract
The Quaternary deposits of the Fenland, consisting of silts, clays, and peats, offer several problems of correlation. Large exposures of these beds have been rare, and hitherto no attempt at dating individual beds has been made, although from the descriptive point of view the whole of the Fenland deposits were dealt with very fully by Skertchley in 1877 (1).
Publisher
Cambridge University Press (CUP)
Reference8 articles.
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